Boaz Nicholas C, Bell Seth R, Groves John T
Department of Chemistry, Princeton University , Princeton, New Jersey 08544, United States.
J Am Chem Soc. 2015 Mar 4;137(8):2875-85. doi: 10.1021/ja508759t. Epub 2015 Feb 17.
Ferryl porphyrins, P-Fe(IV)═O, are central reactive intermediates in the catalytic cycles of numerous heme proteins and a variety of model systems. There has been considerable interest in elucidating factors, such as terminal oxo basicity, that may control ferryl reactivity. Here, the sulfonated, water-soluble ferryl porphyrin complexes tetramesitylporphyrin, oxoFe(IV)TMPS (FeTMPS-II), its 2,6-dichlorophenyl analogue, oxoFe(IV)TDClPS (FeTDClPS-II), and two other analogues are shown to be protonated under turnover conditions to produce the corresponding bis-aqua-iron(III) porphyrin cation radicals. The results reveal a novel internal electromeric equilibrium, P-Fe(IV)═O ⇆ P(+)-Fe(III)(OH2)2. Reversible pKa values in the range of 4-6.3 have been measured for this process by pH-jump, UV-vis spectroscopy. Ferryl protonation has important ramifications for C-H bond cleavage reactions mediated by oxoiron(IV) porphyrin cation radicals in protic media. Both solvent O-H and substrate C-H deuterium kinetic isotope effects are observed for these reactions, indicating that hydrocarbon oxidation by these oxoiron(IV) porphyrin cation radicals occurs via a solvent proton-coupled hydrogen atom transfer from the substrate that has not been previously described. The effective FeO-H bond dissociation energies for FeTMPS-II and FeTDClPS-II were estimated from similar kinetic reactivities of the corresponding oxoFe(IV)TMPS(+) and oxoFe(IV)TDClPS(+) species to be ∼92-94 kcal/mol. Similar values were calculated from the two-proton P(+)-Fe(III)(OH2)2 pKa(obs) and the porphyrin oxidation potentials, despite a 230 mV range for the iron porphyrins examined. Thus, the iron porphyrin with the lower ring oxidation potential has a compensating higher basicity of the ferryl oxygen. The solvent-derived proton adds significantly to the driving force for C-H bond scission.
铁卟啉,P-Fe(IV)═O,是众多血红素蛋白和各种模型体系催化循环中的核心反应中间体。人们对阐明可能控制铁卟啉反应活性的因素,如末端氧的碱性,有着浓厚的兴趣。在此,磺化的水溶性铁卟啉配合物四甲基卟啉、氧代铁(IV)TMPS(FeTMPS-II)、其2,6-二氯苯基类似物氧代铁(IV)TDClPS(FeTDClPS-II)以及其他两种类似物在周转条件下被质子化,生成相应的双水合铁(III)卟啉阳离子自由基。结果揭示了一种新的内部电子互变异构平衡,P-Fe(IV)═O ⇆ P(+)-Fe(III)(OH2)2。通过pH跃变、紫外-可见光谱法测得该过程的可逆pKa值在4-6.3范围内。在质子介质中,铁卟啉质子化对氧代铁(IV)卟啉阳离子自由基介导的C-H键裂解反应有重要影响。对于这些反应,观察到了溶剂O-H和底物C-H的氘动力学同位素效应,这表明这些氧代铁(IV)卟啉阳离子自由基对烃的氧化是通过溶剂质子耦合氢原子从底物转移实现的,这是此前未曾描述过的。根据相应的氧代铁(IV)TMPS(+)和氧代铁(IV)TDClPS(+)物种的相似动力学反应活性,估计FeTMPS-II和FeTDClPS-II的有效FeO-H键解离能约为92-94 kcal/mol。尽管所研究的铁卟啉有230 mV的范围,但从双质子P(+)-Fe(III)(OH2)2的pKa(obs)和卟啉氧化电位计算出了相似的值。因此,具有较低环氧化电位的铁卟啉其铁卟啉氧的碱性相应较高。溶剂衍生的质子显著增加了C-H键断裂的驱动力。